The Bronte Creek bridge in 1936, built as part of The Middle Road, now known as the Queen Elizabeth Way. The original iron truss bridge from the country lane is in the foreground.

Bronte Creek is a waterway in the Lake Ontario watershed of Ontario Canada. It runs through Hamilton and Halton Region, with its source near Morriston[1] (south of the intersection of Highway 6 and Highway 401), passing Bronte Creek Provincial Park, on its way to Lake Ontario at Bronte Harbour in Oakville, where the creek is also known as Twelve Mile Creek. Bronte takes its name from the title of the Duke of Bronté held by Horatio Nelson.[2]

Bronte Creek in Ojibwe is "Eshkwesing-ziibi",[3] "Esqui-sink", "Eshkwessing", "ishkwessin", and "Asquasing" ("that which lies at the end").[4][5][6] [7]

History

A village site associated with the Neutral people and located on the east bank of the creek, the Hood site, was excavated in 1977.[8]: 47 

Geology

Just south of the Queen Elizabeth Way at the Bronte Road exit, the creek has exposed an outcrop of Queenston Formation red shale with narrow, greenish layers of calcareous sandstone and silty bioclastic carbonate.[9]

See also

References

  1. ^ "Creek Locations". Habitats of Hamilton and Halton. Hamilton Naturalists' Club. Archived from the original on 14 December 2012.
  2. ^ "Origins of bronte™ | Bronte™ Collection".
  3. ^ Translate Ojibwe, Ojibwe-English Dictionary, "Eshkwesing-ziibi"Link
  4. ^ "French Sketch Map, c. 1760". Archived from the original on 2014-04-19. Retrieved 2012-02-22.
  5. ^ Baraga, Frederic (1882). A dictionary of the Otchipwe language, explained in English: Part II ..., Part 2. Retrieved 2012-02-22.
  6. ^ FREELANG Ojibwe-English and English-Ojibwe online dictionary
  7. ^ Smith, Donald (2013). Sacred Feathers: The Reverend Peter Jones (Kahkewaquonaby) and the Mississauga Indians. University of Toronto Press. p. 49. ISBN 978-1-4426-1563-2.
  8. ^ Fitzgerald, W. R. (1979). "The Hood Site: Longhouse Burials in an Historic Neutral Village" (PDF). Ontario Archaeology. Ontario Archaeological Society. 32: 43–60.
  9. ^ Brogly, P. J.; I. P. Martini; G. V. Middleton (1998). "The Queenston Formation: shale-dominated, mixed terrigenous-carbonate deposits of Upper Ordovician, semiarid, muddy shores in Ontario, Canada". Canadian Journal of Earth Sciences. 35 (6): 702–719. Bibcode:1998CaJES..35..702B. doi:10.1139/cjes-35-6-702.


43°23′31″N 79°42′51″W / 43.39194°N 79.71417°W / 43.39194; -79.71417


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